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Multiple high-grade crystalline domes across the Pamir contain Barrovian facies-series metapelites with peak metamorphic assemblages of garnet+kyanite±staurolite+biotite+oligoclase±K-white mica. Thermobarometry yields pressures of 6.5–8.2kbar and temperatures of 600–650°C for the Kurgovat dome in the northwestern Pamir, 9.4kbar and 588°C for the west-central Yazgulom dome, 9.1–11.7kbar and 700–800°C...
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